Science Source
Breakup of the Larsen B Ice Shelf triggered by chain reaction drainage of supraglacial lakes
- States that the explosive disintegration of the Larsen B Ice Shelf poses two unresolved questions:
- What process:
- (1) set a horizontal fracture spacing sufficiently small to predispose the subsequent ice shelf fragments to capsize?
- (2) synchronized the widespread drainage of >2750 supraglacial meltwater lakes observed in the days prior to break up?
- What process:
- Answers both questions through analysis of the ice shelf's elastic flexure response to the supraglacial lakes on the ice shelf prior to break up
- Analysis suggests that drainage of a single lake can cause neighboring lakes to drain, which, in turn, causes farther removed lakes to drain
- Concludes that such self-stimulating behavior can account for the sudden, widespread appearance of a fracture system capable of driving explosive break up
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